用SEBAL法估算Zatta (Yamoussoukro-Cô the d '科特迪瓦)灌溉水稻周长的实际蒸散量

Junias Léandre Kra, Moïse Botou Adahi, Brice Arthur Konan-Waidhet, Jean-Yves Konan N’Guessan, Joël Doyéré Koné, Emmanuel Nogbou Assidjo
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摘要

本研究采用SEBAL (Surface Energy Balance Algorithm for Land)模型绘制了亚穆苏克罗省(Côte d ' vovoire)实际蒸散量的时空分布。与该国其他地区一样,亚穆苏克罗地区也面临着蒸散现象。这是一个非常重要的组成部分,在水平衡中起作用,也在农业作物需水量的计算中起作用。因此,其估算在水资源,特别是农业用水的合理管理研究中具有至关重要的意义。本研究的目的是分析实际蒸散发(AET)随土地覆盖和土地利用的时空分布特征。方法基于SEBAL模型,利用遥感(Landsat 8_OLI/TIRS)和气候数据估算实际蒸散量,分析AET的时空分布。结果表明:2019年12月—2020年2月,AET变化范围为0 ~ 5.44 mm/d,平均值为4.92 mm/d;水体平均值最高(4.90 mm/d),淹水植被平均值最高(4.88 mm/d),居民区平均值最低(2.04 mm/d)。此外,结果表明SEBAL模式与FAO-Penman-Monteith方法之间的差异很小,所有卫星图像的平均RMSE为0.36 mm/day。该研究表明,遥感技术在扎塔灌区水稻空间蒸散特征和估算方面具有相当大的潜力。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Estimation of the Actual Evapotranspiration by the SEBAL Method in the Irrigated Rice Perimeter of Zatta (Yamoussoukro—Côte d’Ivoire)
In this study, the SEBAL (Surface Energy Balance Algorithm for Land) model was used to map the spatio-temporal distribution of actual evapotranspiration in the Yamoussoukro department (Côte d’Ivoire). Like other regions of the country, the Yamoussoukro district is confronted with the phenomenon of evapotranspiration (ET). This is a very important component that comes into play in the water balance but also in the calculation of the water needs of agricultural crops. Consequently, its estimation is of paramount importance in research related to the rational management of water resources, particularly agricultural water. The objective of this study was to analyze the spatio-temporal distribution of actual evapotranspiration (AET) as a function of land cover and land use. The methodology used is based on the SEBAL model which uses remote sensing (Landsat 8_OLI/TIRS) and climatic data to estimate actual evapotranspiration and analyze the spatio-temporal distribution of AET. The results reveal that the AET varied from 0 to 5.44 mm/day over the period from December 2019 to February 2020 with an average value of 4.92 mm/day. The highest average values occurred for water bodies (4.90 mm/day) and flooded vegetation (4.88 mm/day) while the lowest values occurred in residential areas (2.04 mm/day). Furthermore, the results show that the difference between the SEBAL model and the FAO-Penman-Monteith method is minimal with an average RMSE of 0.36 mm/day for all the satellite images. This study demonstrates the considerable potential of remote sensing for the characterization and estimation of spatial evapotranspiration in the Zatta irrigated rice-growing area.
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